南岭地区温公岩体的岩石成因及其构造指示

甘成势; 王岳军; 蔡永丰; 刘汇川; 张玉芝; 宋菁菁; 郭小飞

doi:10.3799/dqkx.2016.002

Volume 41 Issue 1

Jan. 2016

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Article Navigation > Earth Science > 2016 > 41(1): 17-34

Gan Chengshi, Wang Yuejun, Cai Yongfeng, Liu Huichuan, Zhang Yuzhi, Song Jingjing, Guo Xiaofei, 2016. The Petrogenesis and Tectonic Implication of Wengong Intrusion in the Nanling Range. Earth Science, 41(1): 17-34. doi: 10.3799/dqkx.2016.002

Citation:

Gan Chengshi, Wang Yuejun, Cai Yongfeng, Liu Huichuan, Zhang Yuzhi, Song Jingjing, Guo Xiaofei, 2016. The Petrogenesis and Tectonic Implication of Wengong Intrusion in the Nanling Range. Earth Science, 41(1): 17-34. doi: 10.3799/dqkx.2016.002

Citation:

Gan Chengshi, Wang Yuejun, Cai Yongfeng, Liu Huichuan, Zhang Yuzhi, Song Jingjing, Guo Xiaofei, 2016. The Petrogenesis and Tectonic Implication of Wengong Intrusion in the Nanling Range. Earth Science, 41(1): 17-34. doi: 10.3799/dqkx.2016.002

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The Petrogenesis and Tectonic Implication of Wengong Intrusion in the Nanling Range

doi: 10.3799/dqkx.2016.002

1.
State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
2.
School of Earth Science and Geological Engineering, Sun Yat-Sen University, Key Laboratory of Mineral Resources and Geological Process of Guangdong, Guangzhou 510275, China
3.
University of Chinese Academy of Sciences, Beijing 100049, China
4.
College of Geosciences, Guilin University of Technology, Guilin 541004, China

Received Date: 2015-09-30
Publish Date: 2016-01-15

Abstract

Abstract

The early Yanshanian geology of southeastern China is characterized by widespread igneous rocks, especially granites. However, the petrogenesis and tectonic implication of these granites in South China remain highly controversial. The A-type granites are the important carrier for better understanding the tectonic evolution of the South China block since the formation is commonly related to extensional tectonic setting. In this study, a set of new zircon U-Pb geochronological, elemental and Sr-Nd-Hf isotopic data is presented for the Wengong A-type granite in eastern Nanling range in northern Guangdong Province. Laser zircon U-Pb dating for the Wengong granitic sample give a weighted mean age of 196.9±4.4 Ma and in-situ zircon ε_Hf(t) values ranging from +2.1 to +7.7. Their whole rock ε_Nd(t) values range from -2.7 to -0.5. The Wengong granites are enriched in SiO₂ (69.22%-76.33%) and total alkalis (7.77%-8.35%). They are metaluminous-peraluminous with A/CNK values ranging from 0.95 to 1.10. These samples have high rare earth element contents, FeOt/MgO (4.40-9.75) and 10 000×Ga/Al ratios (2.9-3.3), as well as significant Sr, Ti and Eu negative anomalies. Based on these geochemical data, it is proposed that the Wengong granites originated from mafic lower crust in response to the earliest Jurassic extensional setting. In combination with available data, it is inferred that the A-type granites in the Nanling range predominantly formed at 196-156 Ma, suggesting an early Yanshanian extensional event in SE China. These A-type granites probably formed in intra-plated extensional environment, indicating the transformation from Paleotethyan to Paleopacific domain after earliest Jurassic.
- Wengong A-type granite,
- Nanling range,
- zircon U-Pb age,
- Sr-Nd-Hf isotope,
- petrology

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References(110)

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The Petrogenesis and Tectonic Implication of Wengong Intrusion in the Nanling Range

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